{"id":184,"date":"2024-11-18T10:30:17","date_gmt":"2024-11-18T10:30:17","guid":{"rendered":"https:\/\/lter.sav.sk\/?page_id=184"},"modified":"2025-03-05T16:22:50","modified_gmt":"2025-03-05T16:22:50","slug":"jalovecka-dolina","status":"publish","type":"page","link":"https:\/\/lter.sav.sk\/index.php\/lokality-a-platformy\/jalovecka-dolina\/","title":{"rendered":"Jaloveck\u00e1 dolina"},"content":{"rendered":"\n<p><strong><ins>DEIMS.iD:<\/ins><\/strong> <a href=\"Https:\/\/deims.org\/e13f1146-b97a-4bc5-9bc5-65322379a567\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/deims.org\/e13f1146-b97a-4bc5-9bc5-65322379a567<\/a><br><strong>Koordin\u00e1tor lokality<\/strong>: <a href=\"http:\/\/www.uh.sav.sk\/sk-sk\/\">\u00dastav krajinnej ekol\u00f3gie SAV, v.v.i.,<\/a> RNDr. \u013dubo\u0161 Halada, CSc., <br><strong>Partnersk\u00e9 organiz\u00e1cie:<\/strong> <a href=\"http:\/\/www.uh.sav.sk\/sk-sk\/ ; https:\/\/mendelu.cz\/\">\u00dastav hydrol\u00f3gie SAV, v.v.i., Mendelova univerzita v Brne<\/a><br><\/p>\n\n\n\n<div class=\"wp-block-group alignwide is-content-justification-center is-nowrap is-layout-flex wp-container-core-group-is-layout-94bc23d7 wp-block-group-is-layout-flex\">\n<p><div class=\"leaflet-map WPLeafletMap\" style=\"height:456px; width:100%;\"><\/div><script>\nwindow.WPLeafletMapPlugin = window.WPLeafletMapPlugin || [];\nwindow.WPLeafletMapPlugin.push(function WPLeafletMapShortcode() {\/*<script>*\/\nvar baseUrl = atob('aHR0cHM6Ly90aWxlLm9wZW5zdHJlZXRtYXAub3JnL3t6fS97eH0ve3l9LnBuZw==');\nvar base = (!baseUrl && window.MQ) ?\n    window.MQ.mapLayer() : L.tileLayer(baseUrl,\n        L.Util.extend({}, {\n            detectRetina: 0,\n        },\n        {\"subdomains\":\"abc\",\"noWrap\":false,\"maxZoom\":19}        )\n    );\n    var options = L.Util.extend({}, {\n        layers: [base],\n        attributionControl: false\n    },\n    {\"zoomControl\":false,\"scrollWheelZoom\":true,\"doubleClickZoom\":false,\"fitBounds\":true,\"minZoom\":0,\"maxZoom\":19,\"maxBounds\":null,\"attribution\":\"<a href=\\\"http:\\\/\\\/leafletjs.com\\\" title=\\\"A JS library for interactive maps\\\">Leaflet<\\\/a>; \\u00a9 <a href=\\\"http:\\\/\\\/www.openstreetmap.org\\\/copyright\\\">OpenStreetMap<\\\/a> contributors\"},\n    {});\nwindow.WPLeafletMapPlugin.createMap(options).setView([49.2169072,19.6714053],12);});<\/script> <script>\nwindow.WPLeafletMapPlugin = window.WPLeafletMapPlugin || [];\nwindow.WPLeafletMapPlugin.push(function WPLeafletMarkerShortcode() {\/*<script>*\/\nvar map = window.WPLeafletMapPlugin.getCurrentMap();\nvar group = window.WPLeafletMapPlugin.getCurrentGroup();\nvar marker_options = window.WPLeafletMapPlugin.getIconOptions({});\nvar marker = L.marker(\n    [0,0],\n    marker_options\n);\nvar is_image = map.is_image_map;\n    marker.setLatLng( map.getCenter() );\nif (marker_options.draggable) {\n    marker.on('dragend', function () {\n        var latlng = this.getLatLng();\n        var lat = latlng.lat;\n        var lng = latlng.lng;\n        if (is_image) {\n            console.log('leaflet-marker y=' + lat + ' x=' + lng);\n        } else {\n            console.log('leaflet-marker lat=' + lat + ' lng=' + lng);\n        }\n    });\n}\nmarker.addTo( group );\nmarker.bindPopup(window.WPLeafletMapPlugin.unescape('Experimental site Salat\u00edn'));window.WPLeafletMapPlugin.markers.push( marker );\n        });<\/script> <script>\nwindow.WPLeafletMapPlugin = window.WPLeafletMapPlugin || [];\nwindow.WPLeafletMapPlugin.push(function WPLeafletkmlShortcode() {\/*<script>*\/\nvar src = 'https:\/\/lter.sav.sk\/wp-content\/uploads\/jal_dol.kml';\nvar default_style = {\"color\":\"white\",\"fillColor\":\"red\"};\nvar rewrite_keys = {\n    stroke : 'color',\n    'stroke-width' : 'weight',\n    'stroke-opacity' : 'opacity',\n    fill : 'fillColor',\n    'fill-opacity' : 'fillOpacity',\n};\n\/\/ htmlspecialchars converts & to \"&amp;\"; 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Le\u017e\u00ed v&nbsp;nadmorsk\u00fdch v\u00fd\u0161kach od 800 m n.m. (\u00fastie Jaloveckej doliny do Liptovskej kotliny) do 2178 m (Ban\u00edkov).&nbsp; Jaloveck\u00e1 dolina sa v&nbsp;hornej \u010dasti rozvetvuje na Bobroveck\u00fa dolinu, Hlbok\u00fa dolinu a&nbsp;dolinu Parichvost. Je to pravdepodobne posledn\u00fd ve\u013ek\u00fd dolinov\u00fd celok na Slovensku, kde nie je vybudovan\u00e1 pr\u00edstupov\u00e1 \u00fadoln\u00e1 lesn\u00e1 cesta. \u00dazemie Jaloveckej doliny je s\u00fa\u010das\u0165ou Tatransk\u00e9ho n\u00e1rodn\u00e9ho parku, juhoz\u00e1padn\u00e1 \u010das\u0165 doliny je chr\u00e1nen\u00e1 v&nbsp;NPR Mn\u00edch a&nbsp;okrajovo sem zasahuje NPR Siv\u00fd vrch.&nbsp;Ide o&nbsp;vysokohorsk\u00fa oblas\u0165, ktor\u00e1 sa vyzna\u010duje najm\u00e4 chladnou kl\u00edmou. Priemern\u00e1 ro\u010dn\u00e1 teplota &nbsp;v&nbsp;obdob\u00ed 1991-2020 bola v&nbsp;\u00fast\u00ed doliny (750 m) 6,6\u00b0C, na \u010cervenci (1500 m n.m.) 3,0 \u00b0C, priemern\u00fd ro\u010dn\u00fd \u00fahrn zr\u00e1\u017eok v&nbsp;\u00fast\u00ed bol 871 mm, na \u010cervenci 1455 mm. Preva\u017en\u00e1 \u010das\u0165 Jaloveckej doliny je budovan\u00e1 kry\u0161talinikom, v&nbsp;ktorom prevl\u00e1daj\u00fa granodiority nad kry\u0161talick\u00fdmi bridlicami &#8211; najm\u00e4 svormi, rulami a migmatitmi. Z\u00e1padn\u00e1 \u010das\u0165 doliny (Siv\u00fd vrch-Babky-Mn\u00edch) je tvoren\u00e1 v\u00e1pencov\u00fdmi horninami &#8211; dolomitmi a v\u00e1pencami druhoh\u00f4r.<\/p>\n\n\n\n<p><\/p>\n\n\n\n<div style=\"width: 700px;\">\n    <div style=\"min-height:400px;\nmargin-left:10px;\nmargin-right: -30px;\n border-radius: 2px; border: 1px solid; rgb(51, 81, 145);\">\n        <div class=\"allmeteo-widget\" data-mg=\"142\" measurands=\"10100,20100,30100,40100,80100,253100\" measurandsNames=\",,,,,soil temperature avg 2cm,soil temperature avg 5cm,\"><\/div>\n    <\/div>\n    <div style=\"font-size: 12px; color: #667; margin-top: 5px;\nmargin-left: 20px; clear: both;\">\n        (kliknut\u00edm na jednotliv\u00e9 riadky d\u00e1t sa zobraz\u00ed graf meran\u00fdch hodn\u00f4t)\n    <\/div>\n<\/div>\n<script type=\"text\/javascript\" src=\"https:\/\/weather.allmeteo.com\/widget\/allmeteo.widget.js\"><\/script>\n<\/div>\n\n\n\n<div class=\"wp-block-group is-nowrap is-layout-flex wp-container-core-group-is-layout-ad2f72ca wp-block-group-is-layout-flex\">\n<p>Lesn\u00e9 a&nbsp;kosodrevinov\u00e9 porasty pokr\u00fdvaj\u00fa preva\u017en\u00fa \u010das\u0165 Jaloveckej doliny. Patria do t\u00fdchto jednotiek potenci\u00e1lnej prirodzenej veget\u00e1cie: Jed\u013eov\u00e9 a jed\u013eovo-smrekov\u00e9 lesy, Smrekov\u00e9 lesy vysokobylinn\u00e9, Smrekovo-smrekovcov\u00e9 lesy a travinn\u00e9 spolo\u010denstv\u00e1, Smrekov\u00e9 lesy \u010du\u010doriedkov\u00e9, Subalp\u00ednske kosodrevinov\u00e9 a travinn\u00e9 kyslomiln\u00e9 spolo\u010denstv\u00e1. Z&nbsp;\u00fazemia je uv\u00e1dzan\u00fd v\u00fdskyt 18 skup\u00edn lesn\u00fdch typov, dominantn\u00fdm typom je jarabinov\u00e1 smre\u010dina (Sorbeto-Piceetum) s&nbsp;v\u00fdmerou 568,9 ha. V Jaloveckej doline sa nach\u00e1dzaj\u00fa hospod\u00e1rske lesy na rozlohe 764,4 ha, v\u00fdmera ochrann\u00fdch lesov je 2 440,9 ha.<br>Alp\u00ednsky stupe\u0148 je tvoren\u00fd preva\u017ene tr\u00e1vnat\u00fdmi spolo\u010denstvami, na kyslom podklade s\u00fa to hlavne vysokohorsk\u00e9 psicov\u00e9 porasty zv\u00e4zu <em>Nardion strictae<\/em>, \u010dast\u00e9 s\u00fa&nbsp; kyslomiln\u00e9 spolo\u010denstv\u00e1 n\u00edzkych kr\u00ed\u010dkov (<em>Loiseleurio-Vaccinetea<\/em>), zriedkavej\u0161ie s\u00fa spolo\u010denstv\u00e1 snehov\u00fdch v\u00fdle\u017e\u00edsk a&nbsp;pol\u00ed\u010dok (<em>Salicetea herbaceae<\/em>), rastlinn\u00e9 spolo\u010denstv\u00e1 pramen\u00edsk (<em>Montoio-Cardaminetea<\/em>)&nbsp;a&nbsp;vysokobylinn\u00e9 spolo\u010denstv\u00e1 vlhk\u00fdch a\u017e mokr\u00fdch n\u00edv (<em>Mulgedio-Aconitetea<\/em>).<\/p>\n<\/div>\n\n\n\n<h3 class=\"wp-block-heading\"><strong>V\u00fdskumn\u00e9 plochy<\/strong><\/h3>\n\n\n\n<p>V&nbsp;roku 2002 bolo v&nbsp;mas\u00edve Salat\u00edna, oblas\u0165 Grapy (49.2168\u00b0N, 19.6714\u00b0E), zalo\u017een\u00fdch 25 trval\u00fdch v\u00fdskumn\u00fdch pl\u00f4ch ve\u013ekosti 2&#215;2 m na experiment\u00e1lne \u0161t\u00fadium vplyvu zv\u00fd\u0161enej depoz\u00edcie dus\u00edka na ekosyst\u00e9m kysl\u00fdch alp\u00ednskych l\u00fak (\u010falej \u201eLokalita Salat\u00edn\u201c). V\u00fdskumn\u00e9 plochy sa nach\u00e1dzaj\u00fa v&nbsp;nadmorskej v\u00fd\u0161ke 1 890-1 900 m, v&nbsp;psicovom poraste zv\u00e4zu <em>Nardion strictae<\/em> na kyslom polo\u017e\u00ed.<\/p>\n\n\n\n<p>Na plochy je ka\u017edoro\u010dne trikr\u00e1t v sez\u00f3ne aplikovan\u00fd dus\u00edk vo forme roztoku NH<sub>4<\/sub>NO<sub>3<\/sub>, resp. fosfor&nbsp;ako roztok KH<sub>2<\/sub>PO<sub>4<\/sub>. Pou\u017eit\u00fdch bolo 5 typov o\u0161etren\u00ed: N2 (2 g N.m<sup>-2<\/sup>.rok<sup>-1<\/sup>), N6 (6 g N.m<sup>-2<\/sup>.rok<sup>-1<\/sup>), N15 (15 g N.m<sup>-2<\/sup>.rok<sup>-1<\/sup>), P (8 g P.m<sup>-2<\/sup>.rok<sup>-1<\/sup>) a&nbsp;C (kontrola, bez pridania chemik\u00e1li\u00ed). O\u0161etrenia s\u00fa 5x replikovan\u00e9, \u0161tyri replik\u00e1cie s\u00fa ur\u010den\u00e9 na nede\u0161truk\u010dn\u00e9 merania, piata aj na de\u0161truk\u010dn\u00e9 merania. V&nbsp;roku 2009 bola ka\u017ed\u00e1 plocha rozdelen\u00e1 na dve polovice ve\u013ekosti 2&#215;1 m, pri\u010dom na jednej polovici sa prestali aplikova\u0165 chemik\u00e1lie, v&nbsp;druhej polovici aplik\u00e1cia chemik\u00e1li\u00ed pokra\u010duje.<\/p>\n\n\n\n<p>Okrem tejto v\u00fdskumnej lokality vykon\u00e1va v&nbsp;Jaloveckej doline \u00dastav hydrol\u00f3gie SAV, v.v.i. dlhodob\u00fd v\u00fdskum hydrologickej bilancie a&nbsp;hydrologick\u00fdch procesov. V&nbsp;r\u00e1mci tohoto v\u00fdskumu s\u00fa od konca 80-tych rokov minul\u00e9ho storo\u010dia prev\u00e1dzkovan\u00e9 meteorologick\u00e9 stanice na Tokarin\u00e1ch v&nbsp;\u00fast\u00ed Jaloveckej doliny (750 m n. m.) a&nbsp;na \u010cervenci (1 500 m n. m.). Od roku 1987 prebiehaj\u00fa merania odtoku z&nbsp;horskej \u010dasti povodia Jaloveck\u00e9ho potoka (limnigraf v&nbsp;nadmorskej v\u00fd\u0161ke 815 m n. m., nad s\u00fatokom Jaloveck\u00e9ho potoka a Sokoln\u00e9ho jarku). Meranie odtoku sa od roku 2011 s&nbsp;preru\u0161eniami vykon\u00e1va aj v&nbsp;z\u00e1vere Bobroveckej doliny a&nbsp;doliny Parichvost. Tieto z\u00e1kladn\u00e9 hydrometeorologick\u00e9 merania s\u00fa dop\u013a\u0148an\u00e9 &nbsp;meraniami zr\u00e1\u017eok, v\u00fd\u0161ky a&nbsp;vodnej hodnoty snehu a vlhkosti p\u00f4dy v&nbsp;Jaloveckej, Bobroveckej a&nbsp;Hlbokej doline. V&nbsp;rokoch 2020 a 2021 boli meteorologick\u00e9 stanice nain\u0161talovan\u00e9 aj v&nbsp;Hlbokej doline (1400 m n. m.) a&nbsp;v Bobroveckej doline (1500 m m. n.m.).<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><strong>\u0160tudovan\u00e9 parametre<\/strong><\/h3>\n\n\n\n<p><strong>Lokalita Salat\u00edn<\/strong><br><strong>Meteorologick\u00e9 parametre<\/strong>: teplota a&nbsp;vlhkos\u0165 vzduchu, zr\u00e1\u017eky, r\u00fdchlos\u0165 a&nbsp;smer vetra, glob\u00e1lne a&nbsp;fotosynteticky akt\u00edvne \u017eiarenie, teplota p\u00f4dy v&nbsp;h\u013abke 5 a&nbsp;20 sm, vlhkos\u0165 p\u00f4dy, vlhkostn\u00fd potenci\u00e1l p\u00f4dy. <strong>P\u00f4dy<\/strong>. <strong>Veget\u00e1cia<\/strong>: bodovou dotykovou met\u00f3dou (100 bodov\/plocha), fytocenologick\u00e9 z\u00e1pisy. <strong>\u017divo\u010d\u00edchy<\/strong>: epigeick\u00e9 bezstavovce (chrob\u00e1ky, pav\u00faky). <strong>Chemizmus <\/strong>p\u00f4dy, p\u00f4dnej vody, biomasy, snehu. <strong>Atmosf\u00e9rick\u00e1 depoz\u00edcia<\/strong> (jedna sez\u00f3na): pH, konduktivita, kati\u00f3ny H+, NH4+, Al3+, K+, Na+, Ca+, Mg+, &nbsp;&nbsp;&nbsp;ani\u00f3ny Cl-, NO3-, a&nbsp; SO4-. Mikrobi\u00e1lna aktivita (iontomeni\u010de). Fenol\u00f3gia \u2013 fenokamera.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><strong>V\u00fdsledky a \u00fadaje<\/strong><\/h3>\n\n\n\n<p>Pravdepodobne najd\u00f4le\u017eitej\u0161\u00ed v\u00fdsledok z&nbsp;v\u00fdskumu na lokalite Salat\u00edn formulovali Bowman et al. (2008) nasledovne:<br>\u201eResults from a&nbsp;nitrogen deposition experiment suggests that a long legacy of acid deposition in the Western Tatra Mountains of Slovakia has pushed soils to a new threshold of acidification usually associated with acid mine drainage soils. We show that increases in nitrogen deposition in the region result in a depletion of both base cations and soluble aluminium, and an increase in extractable iron concentrations. In conjunction with this, we observe a nitrogen deposition-induced reduction in the biomass of vascular plants, associated with a decrease in shoot calcium and magnesium concentrations. We suggest that this site, and potentially others in central Europe, have reached a new and potentially more toxic level of soil acidification in which aluminium release is superseded by iron release into soil water\u201c.<\/p>\n\n\n\n<p>Teploty a&nbsp;zr\u00e1\u017eky z&nbsp;lokality Salat\u00edn:<\/p>\n\n\n\n<p><a href=\"https:\/\/deims.org\/dataset\/122e06fb-11f3-43a7-abc5-067bb302c92b\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/deims.org\/dataset\/122e06fb-11f3-43a7-abc5-067bb302c92b<\/a><br><a href=\"https:\/\/deims.org\/dataset\/84e13ed2-e353-4e1a-abb3-2cf5d596007e\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/deims.org\/dataset\/84e13ed2-e353-4e1a-abb3-2cf5d596007e<\/a><br>Teplota vzduchu, zr\u00e1\u017eky, vlhkos\u0165 p\u00f4dy, r\u00fdchlos\u0165 vetra, slne\u010dn\u00e9 \u017eiarenie a&nbsp;v\u00fd\u0161ka snehu na staniciach \u00dastavu hydrol\u00f3gie SAV, v. v. i.:<br><a href=\"http:\/\/147.213.100.3:81\/meteostations\/EHZMeteoStations.pdf\">http:\/\/147.213.100.3:81\/meteostations\/EHZMeteoStations.pdf<\/a><br><a href=\"http:\/\/www.emsbrno.cz\/p.axd\/en\/Hlbok%C3%A1.dolina_s_.Z%C3%A1padn%C3%A9.Tatry_s_.1400.m.UHSAV.html\">http:\/\/www.emsbrno.cz\/p.axd\/en\/Hlbok%C3%A1.dolina_s_.Z%C3%A1padn%C3%A9.Tatry_s_.1400.m.UHSAV.html<\/a> <a href=\"http:\/\/www.emsbrno.cz\/p.axd\/en\/Bobroveck%C3%A1.dolina_s_.Z%C3%A1padn%C3%A9.Tatry_s_.1500.m.UHSAV.html\">http:\/\/www.emsbrno.cz\/p.axd\/en\/Bobroveck%C3%A1.dolina_s_.Z%C3%A1padn%C3%A9.Tatry_s_.1500.m.UHSAV.html<\/a><\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><strong>Hist\u00f3ria v\u00fdskumu<\/strong><\/h3>\n\n\n\n<p>\u00dastav hydrol\u00f3gie SAV zalo\u017eil v roku 1986 V\u00fdskumn\u00fa z\u00e1klad\u0148u pre horsk\u00fa hydrol\u00f3giu&nbsp;v Liptovskom Mikul\u00e1\u0161i, ktorej v\u00fdskumn\u00fdm \u00fazem\u00edm je povodie Jaloveck\u00e9ho potoka. Hlavnou n\u00e1pl\u0148ou pracoviska je v\u00fdskum zlo\u017eiek vodnej bilancie v&nbsp;hor\u00e1ch a v\u00fdskum hydrologick\u00fdch procesov podmie\u0148uj\u00facich tvorbu vodn\u00fdch zdrojov a&nbsp;odtoku. Napriek bohatej hist\u00f3rii hydrologick\u00e9ho v\u00fdskumu v&nbsp;mal\u00fdch povodiach na Slovensku (Holko et al., 2024), je v&nbsp;s\u00fa\u010dasnosti povodie Jaloveck\u00e9ho potoka jedin\u00fdm horsk\u00fdm povod\u00edm na Slovensku, v&nbsp;ktorom tak\u00fdto v\u00fdskum prebieha. &nbsp;Zariadenia umiestnen\u00e9 v&nbsp;Jaloveckej doline s\u00fa op\u00edsan\u00e9 vy\u0161\u0161ie v&nbsp;\u010dasti \u201eV\u00fdskumn\u00e9 plochy\u201c. Stru\u010dn\u00fd preh\u013ead rie\u0161enej problematiky a&nbsp;v\u00fdsledkov monitoringu hydrologickej bilancie a&nbsp;v\u00fdskumu tvorby odtoku, akumul\u00e1cie a&nbsp;topenia snehu je uveden\u00fd v&nbsp;nieko\u013ek\u00fdch kapitol\u00e1ch monografie Halmov\u00e1 a&nbsp;Kov\u00e1\u010dov\u00e1 (2018) a v publik\u00e1cii Holko et al. (2021). V&nbsp;posledn\u00fdch rokoch sa v\u00fdskum orientoval aj na z\u00edskavanie \u00fadajov pre hodnotenie vplyvu odumierania lesa na hydrologick\u00fd cyklus (Holko et al., 2022, Jan\u010do et al. 2024) a na overovanie vyu\u017eite\u013enosti \u00fadajov, z\u00edskavan\u00fdch z&nbsp;dia\u013ekov\u00e9ho prieskumu Zeme (Sleziak et al., 2023, 2025).<\/p>\n\n\n\n<p>V&nbsp;rokoch 1990-1992 \u0161tudoval Jaloveck\u00fa dolinu t\u00edm \u00dastavu krajinnej ekol\u00f3gie SAV v&nbsp;r\u00e1mci grantov\u00e9ho projektu \u010d. 730 \u201ePriestorov\u00e9&nbsp; a&nbsp; \u010dasov\u00e9&nbsp; ekologick\u00e9 \u0161trukt\u00fary a procesy&nbsp; v&nbsp; \u00fadolnom&nbsp; syst\u00e9me&nbsp; vysokohorsk\u00e9ho pohoria Z\u00e1padn\u00fdch Karp\u00e1t\u201c. Ved\u00facim projektu bol RNDr. Juraj Hre\u0161ko, CSc., v projekte sa \u0161tudovala krajinn\u00e1 \u0161trukt\u00fara, geomorfologick\u00e9 procesy, p\u00f4dne pomery, veget\u00e1cia a&nbsp;vybran\u00e9 skupiny \u017eivo\u010d\u00edchov (pav\u00faky, drobn\u00e9 zemn\u00e9 cicavce, vt\u00e1ky).<\/p>\n\n\n\n<p>V&nbsp;rokoch 2002-2005 bola zalo\u017een\u00e1 v\u00fdskumn\u00e1 lokalita Salat\u00edn v&nbsp;r\u00e1mci projektu National Science Foundation (USA) NSF-0112281 \u201eResponsiveness of alpine vegetation to N inputs &#8211; A Comparison Between Central European and North American Sites\u201c. Ved\u00facim projektu bol Prof. William D. Bowman, rie\u0161ite\u013esk\u00fdmi organiz\u00e1ciami University of Colorado, Boulder, CO, USA, \u00dastav krajinnej ekol\u00f3gie SAV a&nbsp; \u00dastav hydrol\u00f3gie SAV. Na lokalite Salat\u00edn bolo zalo\u017een\u00fdch a&nbsp;trvalo ozna\u010den\u00fdch 25 trval\u00fdch v\u00fdskumn\u00fdch pl\u00f4ch, in\u0161talovala sa meteorologick\u00e1 stanica, za\u010dalo sa s&nbsp;aplik\u00e1ciou chemik\u00e1li\u00ed, zaznamen\u00e1vala sa veget\u00e1cia, \u0161tudovali sa epigeick\u00e9 bezstavovce, v&nbsp;jednej sez\u00f3ne sa merala mokr\u00e1 atmosf\u00e9rick\u00e1 depoz\u00edcia, urobili sa odbery biomasy, p\u00f4dnej vody, p\u00f4dy, snehu a&nbsp;n\u00e1sledne chemick\u00e9 anal\u00fdzy vzoriek.<\/p>\n\n\n\n<p>Po skon\u010den\u00ed projektu NSF bol v\u00fdskum na lokalite Salat\u00edn financovan\u00fd z\u00a0viacer\u00fdch projektov, preva\u017ene projektov agent\u00fary VEGA, v\u00a0niektor\u00fdch rokoch nebol projektovo kryt\u00fd a\u00a0financoval sa z\u00a0in\u0161titucion\u00e1lnych prostriedkov \u00daKE SAV. V\u00a0roku 2008 sa lokalita Jaloveck\u00e1 dolina stala s\u00fa\u010das\u0165ou siete LTER Slovensko, koordin\u00e1torom v\u00fdskumu na lokalite je \u013dubo\u0161 Halada. Kontaktnou osobou oh\u013eadne hydrologick\u00e9ho v\u00fdskumu v\u00a0povod\u00ed Jaloveck\u00e9ho potoka, ktor\u00fd v\u00fdkon\u00e1va \u00dastav hydrol\u00f3gie SAV, v.v.i., \u00a0je Michal Danko.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p><a id=\"_msocom_1\"><\/a><\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><strong>Publik\u00e1cie<\/strong><\/h3>\n\n\n\n<p>Ballo, M., Holko, L. (editori.), 2015: Divo\u010dina pod Salat\u00ednom. &#8211; REPROservis &#8211; DTP \u0161t\u00fadio &amp; tla\u010diare\u0148, Liptovsk\u00fd Mikul\u00e1\u0161, 344 str\u00e1n &#8211; <a href=\"https:\/\/www.researchgate.net\/publication\/304215493_Divocina_pod_Salatinom\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/www.researchgate.net\/publication\/304215493_Divocina_pod_Salatinom<\/a><\/p>\n\n\n\n<p>Bowman, W.D., Cleveland, C.C., Halada, \u013d., Hre\u0161ko, J., Baron, J.S., 2008: Negative impact of nitrogen deposition on soil buffering capacity. &#8211; Nature Geoscience 1: 767-770. &#8211; <a href=\"https:\/\/doi.org\/10.1038\/ngeo339\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1038\/ngeo339<\/a><\/p>\n\n\n\n<p>Bowman, W.D., Halada, \u013d., Hre\u0161ko, J., Cleveland, C.C., Baron, J.S., Murgel, J., 2014: How Much is too Much? Nitrogen Critical Loads and Eutrophication and Acidification in Oligotrophic Ecosystems. \u2013 In: Sutton, M.A., Mason, K.E., Sheppard, L.J., Sverdrup, H., Haeuber, R., Hicks, W.K. (eds.): Nitrogen Deposition, Critical Loads and Biodiversity. Springer Verlag, Dordrecht: 305-310&nbsp;&nbsp;ISBN:&nbsp;978-94-007-7938-9 &#8211; <a href=\"https:\/\/doi.org\/10.1007\/978-94-007-7939-6_32\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1007\/978-94-007-7939-6_32<\/a><\/p>\n\n\n\n<p>Halada, \u013d., David, S., Halabuk, A., 2009: Vegetation Structure and Aboveground Biomass at Mt. Salat\u00edn Long-Term Ecological Research Site, the West Tatra Mts., Slovakia. \u2013 Ekol\u00f3gia (Bratislava) 28, 2: 113-126.&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; <a href=\"https:\/\/publikacie.uke.sav.sk\/taxonomy\/term\/718\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/publikacie.uke.sav.sk\/taxonomy\/term\/718<\/a><\/p>\n\n\n\n<p>Halada, \u013d., Z\u00e1hora, J., Gajdo\u0161, P., Hre\u0161ko, J., T\u016fma, I., David, S., Mojses, M., Bug\u00e1r, G., Koh\u00fat F., Bolti\u017eiar, M., Majzlan, O., 2016: Alp\u00ednske l\u00faky Z\u00e1padn\u00fdch Tatier pod vplyvom dlhodob\u00e9ho zne\u010distenia ovzdu\u0161ia. &#8211; \u017divotn\u00e9 prostredie, Bratislava, 50, 2: 72 \u2013 80 <a href=\"https:\/\/publikacie.uke.sav.sk\/taxonomy\/term\/896\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/publikacie.uke.sav.sk\/taxonomy\/term\/896<\/a><\/p>\n\n\n\n<p>Halmov\u00e1, D., Kov\u00e1\u010dov\u00e1, V. (eds.), 2018: Hydrologick\u00fd v\u00fdskum v&nbsp;podmienkach prebiehaj\u00facej klimatickej zmeny. &#8211; VEDA, Bratislava, 382 str\u00e1n.<\/p>\n\n\n\n<p>Holko, L., Danko, M., Hlav\u010do, J., Kostka, Z., 2016: <a href=\"http:\/\/publikacie.uke.sav.sk\/node\/4032\" target=\"_blank\" rel=\"noreferrer noopener\">Dlhodob\u00e9 \u00fadaje o priebehu vybran\u00fdch klimatick\u00fdch a hydrologick\u00fdch prvkov v povod\u00ed Jaloveck\u00e9ho potoka (Z\u00e1padn\u00e9 Tatry, Liptovsk\u00e1 kotlina)<\/a>. &#8211; \u017divotn\u00e9 prostredie, Bratislava, 50, 2: 81-86. <a href=\"https:\/\/publikacie.uke.sav.sk\/taxonomy\/term\/896\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/publikacie.uke.sav.sk\/taxonomy\/term\/896<\/a><\/p>\n\n\n\n<p>Holko L, Danko M, Sleziak P., 2021: Snowmelt characteristics in a pristine mountain catchment of the Jaloveck\u00fd Creek, Slovakia, over the last three decades. &#8211; Hydrological Processes 35: e14128. <a href=\"https:\/\/doi.org\/10.1002\/hyp.14128\">https:\/\/doi.org\/10.1002\/hyp.14128<\/a><\/p>\n\n\n\n<p>Holko, L., Jan\u010do, M., Danko, M., Sleziak, P., 2022: Influence of forest dieback on the overland flow and isotopic composition of precipitation. &#8211; Acta Hydrologica Slovaca 23, 1: 82 \u2013 88. DOI: 10.31577\/ahs-2022-0023.01.0009<\/p>\n\n\n\n<p>Holko, L., Pek\u00e1rov\u00e1, P., Szolgay, J., Mikl\u00e1nek, P., Babiakov\u00e1, G., 2025: History of hydrological research in Slovakia and its links to water management. Hydrological Sciences Journal 70, 1: 10 \u2013 26. DOI: 10.1080\/02626667.2024.2422532 Jan\u010do, M., Danko, M., Sleziak, P., Holko, L., 2024: Estimation of the leaf area index in a decline spruce forest in the Western Tatra Mountains for determination of rainfall interception. &#8211; Acta Hydrologica Slovaca 25, 1: 106 \u2013 114. DOI: 10.31577\/ahs-2024-0025.01.0012<\/p>\n\n\n\n<p>Jan\u010do, M., Danko, M., Sleziak, P., Holko, L., 2024: Estimation of the leaf area index in a decline spruce forest in the Western Tatra Mountains for determination of rainfall interception. &#8211; Acta Hydrologica Slovaca 25, 1: 106 \u2013 114. DOI: 10.31577\/ahs-2024-0025.01.0012<\/p>\n\n\n\n<p>Lanc\u00fach, P., Hanaj\u00edk, P., 2005: Biomasa mikroorganizmov vo vysokohorsk\u00fdch l\u00fa\u010dnych ekosyst\u00e9moch \/ In: \u017divot v p\u00f4de 6. Zborn\u00edk z medzin\u00e1rodn\u00e9ho semin\u00e1ra. &#8211; ISBN 80-213-1348-X. &#8211; Praha : \u010cesk\u00e1 zem\u011bd\u011blsk\u00e1 univerzita, 2005: 117-120<\/p>\n\n\n\n<p>Lanc\u00fach, P., \u010eugov\u00e1, O., 2006: Vplyv aplik\u00e1cie dus\u00edkat\u00fdch (NH4NO3) a fosfore\u010dn\u00fdch (KH2PO4) hnoj\u00edv na mikrobiotu vysokohorsk\u00fdch l\u00fa\u010dnych ekosyst\u00e9mov. &#8211; In: \u017divot v p\u00f4de 7. Zborn\u00edk z medzin\u00e1rodn\u00e9ho semin\u00e1ra. Bratislava: Univerzita Komensk\u00e9ho, 2006: 204-212.<\/p>\n\n\n\n<p>Pilotto, F., K\u00fchn, I., Adrian, R., Alber, R., Alignier, A., Andrews, Ch., B\u00e4ck, J., Barbaro, L., Beaumont, D., Beenaerts1, N., Benham, S., Boukal, D.S., Camatti, E., Canullo, R., Cardoso, P., Ens, B.J., Everaert, G., Evtimova, V., Garc\u00eda-Gonz\u00e1lez, R., G\u00f3mez Garc\u00eda, D., Grandin, U.,&nbsp; Gutowski, J.M., Hadar, L., Halada, L., Halassy, M., Hummel, H., Huttunen, K.-L., Jaroszewicz, B., Jensen, T.C., Kalivoda, H., Kappel Schmidt, I., Kr\u00f6ncke, I., Leinonen, R., Martinho, F., Meesenburg, H., Meyer, J., Minerbi, S., Monteith, D., Nikolov, B.P., Oro, D., Ozoli\u0146\u0161, D., Padedda, B.M., Pallett, D., Pansera, M., Pardal, M.A., Petriccione, B., Pipan, T., P\u00f6yry, J., Sch\u00e4fer, S.M., Schaub, M., Schneider, S.C., Skuja, A., Soetaert, K., Spri\u0146\u0123e, G., Stanchev, R., Stockan, J. A., Stoll, S., Sundqvist, L., Thimonier, A., Van Hoey, G., Van Ryckegem, G., Visser, M.E., Vorhauser, S., Haase, P. (2020): Meta-analysis of multidecadal biodiversity trends in Europe. \u2013 Nature Communications 11, 1: 3486. <a href=\"https:\/\/doi.org\/10.1038\/s41467-020-17171-y\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1038\/s41467-020-17171-y<\/a><\/p>\n\n\n\n<p>Sleziak, P., Jan\u010do, M., Danko, M., M\u00e9ri, L., Holko, L., 2023: Accuracy of radar-estimated precipitation in a mountain catchment in Slovakia. &#8211; J. Hydrol. Hydromech. 71, 1: 111\u2013122. <a href=\"https:\/\/doi.org\/10.2478\/johh-2022-0037\">https:\/\/doi.org\/10.2478\/johh-2022-0037<\/a><\/p>\n\n\n\n<p>Sleziak, P., Danko, M., Jan\u010do, M., Holko, L., Greimeister-Pfeil, I., Vreugdenhil, M., Parajka, J., 2025: Accuracy of ASCAT-DIREX Soil Moisture Mapping in a Small Alpine Catchment. &#8211; Water 17, 1, 49. <a href=\"https:\/\/doi.org\/10.3390\/w17010049\">https:\/\/doi.org\/10.3390\/w17010049<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>DEIMS.iD: https:\/\/deims.org\/e13f1146-b97a-4bc5-9bc5-65322379a567Koordin\u00e1tor lokality: \u00dastav krajinnej ekol\u00f3gie SAV, v.v.i., RNDr. \u013dubo\u0161 Halada, CSc., Partnersk\u00e9 organiz\u00e1cie: \u00dastav hydrol\u00f3gie SAV, v.v.i., Mendelova univerzita v Brne Pr\u00edrodn\u00e9 pomery Komplex Jaloveckej doliny sa nach\u00e1dza v&nbsp;z\u00e1padnej \u010dasti Z\u00e1padn\u00fdch Tatier, dolinov\u00fd syst\u00e9m je orientovan\u00fd na juh. Le\u017e\u00ed v&nbsp;nadmorsk\u00fdch v\u00fd\u0161kach od 800 m n.m. (\u00fastie Jaloveckej doliny do Liptovskej kotliny) do 2178 m&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":85,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_kad_post_transparent":"","_kad_post_title":"","_kad_post_layout":"","_kad_post_sidebar_id":"","_kad_post_content_style":"default","_kad_post_vertical_padding":"","_kad_post_feature":"","_kad_post_feature_position":"","_kad_post_header":false,"_kad_post_footer":false,"_kad_post_classname":"","footnotes":""},"class_list":["post-184","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/184","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/comments?post=184"}],"version-history":[{"count":29,"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/184\/revisions"}],"predecessor-version":[{"id":570,"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/184\/revisions\/570"}],"up":[{"embeddable":true,"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/85"}],"wp:attachment":[{"href":"https:\/\/lter.sav.sk\/index.php\/wp-json\/wp\/v2\/media?parent=184"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}